The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: Implications for deeply subducted sediments

Geochimica et Cosmochimica Acta

Volumn 60, Issue 21, 1996, Pages 4133-4150

  Domanik, Kenneth J ^a   Holloway, John R ^a  

^a ARIZONA STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ARC MAGMA; MINERAL COMPOSITION; MUSCOVITE; PHENGITE; STABILITY; SUBDUCTED SEDIMENT;

EID: 0030440665     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(96)00241-4     Document Type: Article

References (63)

1. Bebout G. E., Ryan J. G., and Leeman W. P. (1993) B-Be systematics in subduction-related metamorphic rocks: Characterization of the subducted component. Geochim. Cosmochim. Acta 56, 2839-2849.
2. Bertka C. M. and Fei Y. (1996) Mineralogy of the Martian interior up to core-mantle boundary pressures. J. Geophys. Res (in press).
3. Burt D. M. (1988) Vector representation of phyllosilicate compositions. Rev. Mineral. 19, 561-599.
4. Coats R. R. (1962) Magma type and crustal structure in the Aleutian arc. Geophys. Monogr. 6, 92-109.
5. Comodi P. and Zanazzi P. F. (1995) High-pressure structural study of muscovite. Phys. Chem. Min. 22, 170-177.
6. Devine J. D., Gardner J. E., Brack H. P., Layne G. D., and Rutherford M. J. (1995) Comparison of microanalytical methods for estimating H2O contents of silicic volcanic glasses. Am. Mineral. 80, 319-328.
7. Domanik K. J. (1992) The distribution of beryllium and boron in high pressure, low temperature minerals. Unpublished M. S. Thesis, Arizona State Univ.
8. Domanik K. J., Hervig R. L., and Peacock S. M. (1993) Beryllium and boron in subduction zone minerals: an ion microprobe study. Geochim. Cosmochim. Acta 57, 4997-5010.
9. Faust J. and Knittle E. (1994) The equation of state, amorphization, and high-pressure phase diagram of muscovite. J. Geophys. Res. 99, 19,785-19,792.
10. Gasparik T. (1989) Transformation of enstatite-diopside-jadeite pyroxenes to garnet. Contrib. Mineral. Petrol. 102, 389-405.
11. Ghent E. D., Black P. M., Brothers R. N., and Stout M. Z. (1987) Eclogites and associated albite-epidote-garnet paragniesses between Yambe and cape Colnett, New Caledonia. J. Petrol. 28, 627-643.
12. Giaramita M. J. and Sorensen S. S. (1994) Primary fluids in low temperature eclogites; evidence from two subduction complexes (Dominican Republic, and California, USA. Contrib. Mineral. Petrol. 117, 279-292.
13. Gill J. (1981) Orogenic Andesites and Plate Tectonics. Springer-Verlag.
14. Green T. H. (1981) Synthetic high-pressure micas compositionally intermediate between the dioctahedral and trioctahedral mica series. Contrib. Mineral. Petrol. 78, 452-458.
15. Green T. H. and Hellman P. L. (1982) Fe-Mg partitioning between coexisting garnet and phengite at high pressure, and comments on a garnet-phengite geothermometer. Lithos 15, 253-266.
16. Guidotti C. V. (1984) Micas in metamorphic rocks. Rev. Mineral. 13, 357-346.
17. 1 muscovite and paragonite. Eur. J. Mineral. 4, 283-297.
18. Harley S. L. and Green D. H. (1981) Petrogenesis of eclogite inclusions in the Moses Rock dyke USA. Tschermaks Mineral. Petrogr. Mitt. 28, 131-155.
19. Hazen R. M. and Wones D. R. (1972) The effects of cation substitution on the physical properties of trioctahedral micas. Amer. Mineral. 58, 103-129.
20. Hazen R. M. and Wones D. R. (1978) Predicted and observed compositional limits to trioctahedral micas. Amer. Mineral. 63, 885-892.
21. Holloway J. R. and Ford C. E. (1975) Fluid absent melting of the fluoro-hydroxy amphibole pargasite to 35 kilobars. Earth Planet. Sci. Lett. 25, 44-48.
22. 2O. Contrib. Mineral. Petrol. 105, 393-402.
23. 2O. Amer. Jour. Sci. 273, 415-427.
24. Irifune T., Ringwood A. E., and Hibberson W. O. (1994) Subduction of continental crust and terrigenous and pelagic sediments: and experimental study. Earth Planet. Sci. Lett. 126, 351-368.
25. Kretz R. (1983) Symbols for rock forming minerals. Amer. Mineral. 68, 277-279.
26. Krogh E. J. and Raheim A. (1978) Temperature and pressure dependence of Fe-Mg partitioning between garnet and phengite with particular reference to eclogites. Contrib. Mineral. Petrol. 66, 75-80.
27. Lesher C. E. and Walker D. (1988) Cumulate maturation and melt migration in a temperature gradient. J. Geophys. Res. 93, 10295-10311.
28. Liu L. (1989) Stability Fields of Mg-pumpellyite composition at high pressures and temperatures. Geophys. Res. Lett. 16, 847-849.
29. Maruyama S. and Liou J. G. (1988) Petrology of Franciscan metabasites along the jadeite-glaucophane type facies, Cazadero, California. J. Petrol. 29, 1-37.
30. 2O (KMASH). Lithos 28, 421-434.
31. Massonne H. J. (1994) P-T evolution of phengite-bearing marbles from the Hellenides. EOS Trans. Amer. Geophys. Union 75, 744.
32. 2O. Neues. Jahrb. Mineral Abh. 153, 177-215.
33. Massonne H. J. and Schreyer W. (1987) Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz. Contrib. Mineral. Petrol. 96, 212-224.
34. Massonne H. J. and Schreyer W. (1989) Stability field of the high-pressure assemblage talc + phengite and two new phengite barometers. Eur. J. Mineral. 1, 391-410.
35. Morris J. D., Leeman W. P., and Tera F. (1990) The subducted component in island arc lavas: constraints from Be isotopes and B-Be systematics. Nature 344, 31-36.
36. Oh C. W. and Liou J. G. (1990) Metamorphic evolution of two different eclogites in the Franciscan Complex, California, USA. Lithos 25, 41-53.
37. Oh C. W., Liou J. G., and Maruyama S. (1991) Low-temperature eclogites and eclogitic schists in Mn-rich metabasites in Ward Creek, California; Mn and Fe effects on the transition between blueschist and eclogite. J. Petrol. 32, 275-302.
38. 2O recycling in subduction zones. Contrib. Mineral. Petrol. 118, 99-108.
39. Peacock S. M., Rushmer T., and Thompson A. B. (1994) Partial melting of subducting oceanic crust. Earth Planet. Sci. Lett. 121, 227-244.
40. Poli S. and Schmidt M. W. (1995) Water transport and release in subduction zones: experimental constraints on basaltic and andesitic systems. J. Geophys. Res. 100, 22299-22314.
41. Schertl H., Schreyer W., and Chopin C. (1991 ) The pyrope-coesite rocks and their country rocks at Parigi, Dora Maira massif, Western Alps: Detailed petrography, mineral chemistry and P-T path. Contrib. Mineral. Petrol. 108, 1-21.
42. Schmidt M. W. (1993) Phase relations and compositions in tonalite as a function of pressure: an experimental study at 650°C. Amer. J. Sci. 293, 1011-1060.
43. Schmidt M. W. (1995a) The stability of phengite and K-metasomatism of the mantle wedge above subduction zones. EOS Trans. Amer. Geophys. Union 76, 537.
44. Schmidt M. W. (1995b) Lawsonite: Upper pressure stability and formation of higher density hydrous phases. Amer. Mineral. 80, 1286-1292.
45. Schmidt M. W. and Poli S. (1994) The stability of lawsonite and zoisite at high pressures: Experiments in CASH to 92 kbar and implications for the presence of hydrous phases in subducted lithosphere. Earth Planet. Sci. Lett. 124, 105-118.
46. Schreyer W., Maresh W. V., Medenbach O., and Baller T. (1986) Calcium-free pumpellyite, a new synthetic hydrous Mg-Al-silicate formed at high pressures. Nature 321, 510-511.
47. Schreyer W., Maresh W. V., Medenbach O., and Baller T. (1987) MgMgAl-pumpellyite: a new hydrous, high-pressure, synthetic silicate resulting from Mg-for-Ca substitution. Terra Cognita 7, 385.
48. 8, at high temperatures and pressures. Amer. Mineral. 49, 1688-1706.
49. Shaw D. M. (1965) Geochemistry of pelitic rocks. III. Major elements and geochemistry. Bull. Geol. Soc. Amer. 67, 919-934.
50. Sorensen S. (1994) Subduction-related K-Rb-Ba metasomatism of high grade melange blocks from California, USA and the Dominican Republic. SUBCON Abstr. Vol., 213-215.
51. Sorensen S. S., Grossman J. N., and Perfit M. R. (1996) Phengitehosted LILE enrichment in eclogite and related rocks: implications for fluid-mediated mass transfer in subduction zones and arc magma genesis. J. Petrol. (in press).
52. Tatsumi Y. (1989) Migration of fluid phases and genesis of basalt magmas in subduction zones. Jour. Geophys. Res. 94,4697-4707.
53. Thompson A. B. (1983) Fluid-absent metamorphism. J. Geo. Soc. London 140, 533-547.
54. Thompson A. B. (1992) Water in the Earth's upper mantle. Nature 358, 295-301.
55. 8. Phy. Chem. Min. 21, 387-391.
56. Vavilov M. A., Sobolev N. V., and Shatskiy V. S. (1991) Micas in diamond-bearing metamorphic rocks of northern Kazakhstan. Doklady Akademii Nauk 319, 466-470.
57. Velde B. (1965) Phengite micas: synthesis, stability, and natural occurrence. Amer. J. Sci. 263, 886-913.
58. 4+ content of natural phengites. Contrib. Mineral. Petrol. 14, 250-258.
59. Wang X., Liou J. G., and Mao H. K. (1989) Coesite-bearing eclogite from the Dabie Mountains in Central China. Geol. 17, 1085-1088.
60. 2: A fully hydrated analogue of topaz. Amer. Mineral. 78, 285-297.
61. Yagi T. and Akimoto S. (1976) Direct determination of coesitestishovite transition by in-situ X-ray measurements. Tectphy. 35, 259-270.
62. 2O system and related metamorphic facies. Amer. J. Sci. Bowen Vol., 569-627.
63. 8 hollandite. Amer. Mineral. 78, 493-499.